抄録
The biological flux and lifetime of methanol in anoxic marine sediments are largely unknown. We herein reported, for the first time, quantitative methanol removal rates in subsurface sediments. Anaerobic incubation experiments with radiotracers showed high rates of microbial methanol consumption. Notably, methanol oxidation to CO2 surpassed methanol assimilation and methanogenesis from CO2/H2 and methanol. Nevertheless, a significant decrease in methanol was not observed after the incubation, and this was attributed to the microbial production of methanol in parallel with its consumption. These results suggest that microbial reactions play an important role in the sources and sinks of methanol in subseafloor sediments.
| 元の言語 | 英語 |
|---|---|
| ページ（範囲） | 190-193 |
| ページ数 | 4 |
| ジャーナル | Microbes and Environments |
| 巻 | 31 |
| 発行部数 | 2 |
| DOI | |
| 出版物ステータス | 出版済み - 6 25 2016 |
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All Science Journal Classification (ASJC) codes
- Ecology, Evolution, Behavior and Systematics
- Soil Science
- Plant Science
これを引用
Biogeochemical cycle of methanol in anoxic deep-sea sediments. / Yanagawa, Katsunori; Tani, Atsushi; Yamamoto, Naoya; Hachikubo, Akihiro; Kano, Akihiro; Matsumoto, Ryo; Suzuki, Yohey.
：: Microbes and Environments, 巻 31, 番号 2, 25.06.2016, p. 190-193.研究成果: ジャーナルへの寄稿 › 記事
}
TY - JOUR
T1 - Biogeochemical cycle of methanol in anoxic deep-sea sediments
AU - Yanagawa, Katsunori
AU - Tani, Atsushi
AU - Yamamoto, Naoya
AU - Hachikubo, Akihiro
AU - Kano, Akihiro
AU - Matsumoto, Ryo
AU - Suzuki, Yohey
PY - 2016/6/25
Y1 - 2016/6/25
N2 - The biological flux and lifetime of methanol in anoxic marine sediments are largely unknown. We herein reported, for the first time, quantitative methanol removal rates in subsurface sediments. Anaerobic incubation experiments with radiotracers showed high rates of microbial methanol consumption. Notably, methanol oxidation to CO2 surpassed methanol assimilation and methanogenesis from CO2/H2 and methanol. Nevertheless, a significant decrease in methanol was not observed after the incubation, and this was attributed to the microbial production of methanol in parallel with its consumption. These results suggest that microbial reactions play an important role in the sources and sinks of methanol in subseafloor sediments.
AB - The biological flux and lifetime of methanol in anoxic marine sediments are largely unknown. We herein reported, for the first time, quantitative methanol removal rates in subsurface sediments. Anaerobic incubation experiments with radiotracers showed high rates of microbial methanol consumption. Notably, methanol oxidation to CO2 surpassed methanol assimilation and methanogenesis from CO2/H2 and methanol. Nevertheless, a significant decrease in methanol was not observed after the incubation, and this was attributed to the microbial production of methanol in parallel with its consumption. These results suggest that microbial reactions play an important role in the sources and sinks of methanol in subseafloor sediments.
UR - http://www.scopus.com/inward/record.url?scp=84975800815&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84975800815&partnerID=8YFLogxK
U2 - 10.1264/jsme2.ME15204
DO - 10.1264/jsme2.ME15204
M3 - Article
AN - SCOPUS:84975800815
VL - 31
SP - 190
EP - 193
JO - Microbes and Environments
JF - Microbes and Environments
SN - 1342-6311
IS - 2
ER -